{"id":90010,"date":"2001-04-05T00:00:00","date_gmt":"2001-04-05T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/mineralizaciones-filonianas-de-bielsa-pirineos-aragoneses-papel-de-los-fluidos-sintectonicos-en-su-genesis\/"},"modified":"2001-04-05T00:00:00","modified_gmt":"2001-04-05T00:00:00","slug":"mineralizaciones-filonianas-de-bielsa-pirineos-aragoneses-papel-de-los-fluidos-sintectonicos-en-su-genesis","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/mineralizaciones-filonianas-de-bielsa-pirineos-aragoneses-papel-de-los-fluidos-sintectonicos-en-su-genesis\/","title":{"rendered":"Mineralizaciones filonianas de bielsa (pirineos aragoneses). papel de los fluidos sintectonicos en su genesis."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Alfonso Yuste Oliete <\/strong><\/h2>\n<p>El objeto de este trabajo ha sido el estudio de los yacimientos minerales que se encuentran en las inmediaciones de bielsa (huesca). En concreto, se ha estudiado tres filones intragran\u00edticos (ana, luc\u00eda y t\u00fanel), otro encajado en el tr\u00edas inferior (montillo) y una serie de peque\u00f1as vetas, tambi\u00e9n intratri\u00e1sicas, que constituyen los indicios de bielsa. Todos ellos son filones de fluorita con cantidades variables de galena, pirita, esfalerita, cuarzo, carbonatos, barita, calcopirita, sulfosales, hematiles, magnetita y arsenopirita.  desde el punto de vista geol\u00f3gico, todos los yacimientos se localizan en la zona axial de los pirineos centrales, que en el \u00e1rea de estudio consiste fundamentalmente en rocas paleozoicas deformadas, sometidas a metamorfimos regional e intru\u00eddas por el plut\u00f3n granodior\u00edtico de bielsa, constituyendo todo este conjunto el basamento herc\u00ednico. Sobre \u00e9ste aparecen discordantemente las areniscas rojas del tri\u00e1sico inferior y sobre \u00e9stas los materiales del tri\u00e1sico medio y superior. Finalmente, sobre el tri\u00e1sico aparecen las calizas del cret\u00e1cico superior. La tect\u00f3nica de mantos alpina (eoceno-mioceno) es la principal responsable de la estructura geol\u00f3gica de la zona. Uno de los accidentes tect\u00f3nicos m\u00e1s importantes en el \u00e1rea de bielsa es el manto de gavarmie, cuya culminaci\u00f3n tiene lugar en la cobertera mesozoica (areniscas rojas del tr\u00edas inferior y calizas del cret\u00e1cico superior), la cual se encuentra entre el basamiento y las l\u00e1minas cabalgantes del manto de gavarnie.  los yacimientos estudiados rellenan fracturas tardihericinicas subverticales de direcci\u00f3n aproximada e-w, probablemente reactivadas durante la orogenia alpina. Como resultado de esta reactivaci\u00f3n, todas las mineralizaciones, excepto los indicios de bielsa, ostentan evidentes signos de deformaci\u00f3n d\u00factil y fr\u00e1gil, consistente en una foliaci\u00f3n mineral\u00f3gica y textural, estructura milon\u00edtica y desarrollo de brechas.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Mineralizaciones filonianas de bielsa (pirineos aragoneses). papel de los fluidos sintectonicos en su genesis.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Mineralizaciones filonianas de bielsa (pirineos aragoneses). papel de los fluidos sintectonicos en su genesis. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Alfonso Yuste Oliete <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Zaragoza<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 04\/05\/2001<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n<h3>Direcci\u00f3n y tribunal<\/h3>\n<ul>\n<li><strong>Director de la tesis<\/strong>\n<ul>\n<li>nieto Gonzalez Fernandez<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Francisco Velasco roldan <\/li>\n<li>Jos\u00e9 Torres ruiz (vocal)<\/li>\n<li>Miguel Orozco fern\u00e1ndez (vocal)<\/li>\n<li>cinta Osacar soriano (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Alfonso Yuste Oliete El objeto de este trabajo ha sido el estudio de los yacimientos minerales que [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"footnotes":""},"categories":[27,953,232,3612,13610],"tags":[187003,187004,4039,9534,21705,28752],"class_list":["post-90010","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-geologia","category-mineralogia","category-yacimientos-minerales","category-zaragoza","tag-alfonso-yuste-oliete","tag-cinta-osacar-soriano","tag-francisco-velasco-roldan","tag-jose-torres-ruiz","tag-miguel-orozco-fernandez","tag-nieto-gonzalez-fernandez"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/90010","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/comments?post=90010"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/90010\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=90010"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=90010"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=90010"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}